[et_pb_section fb_built=\u00a0\u00bb1″ _builder_version=\u00a0\u00bb4.4.7″ custom_padding=\u00a0\u00bb5px|||||\u00a0\u00bb][et_pb_row _builder_version=\u00a0\u00bb4.4.7″ custom_padding=\u00a0\u00bb0px||0px|||\u00a0\u00bb][et_pb_column type=\u00a0\u00bb4_4″ _builder_version=\u00a0\u00bb4.4.7″][et_pb_text _builder_version=\u00a0\u00bb4.4.8″ hover_enabled=\u00a0\u00bb0″ custom_padding=\u00a0\u00bb||59px|||\u00a0\u00bb]<\/p>\n
Was particularly successful, even if it took ten days to run in the system, ceilings of 7,000 to 8,000 m in thermal (most often blue) not being part of the meteorological standards. The forecast was limited to two days, sufficient for our goal, the discovery. The main interest of SkySight in thermals was the forecast in steps of 30 minutes, allowing us to anticipate the beginning and the end of convection because at the tropics, the sun goes down very quickly, at 6 p.m. you have to be on the final glide (120 km), at 8 p.m. it is dark. Of course, the strong point of this software lies in the forecasting of dynamic systems and we did use it, without neglecting the study of general maps of public domain on continental scale, and especially the jet streams, of which it is confirmed once again that their presence is a sufficient condition for the establishment of powerful wave systems.<\/span><\/p>\n [\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=\u00a0\u00bb3_4,1_4″ _builder_version=\u00a0\u00bb4.4.8″][et_pb_column type=\u00a0\u00bb3_4″ _builder_version=\u00a0\u00bb4.4.8″][et_pb_image src=\u00a0\u00bbhttps:\/\/topfly-aero.com\/wp-content\/uploads\/2020\/06\/191107-15.30-SS-THERMALS-MAP.png\u00a0\u00bb title_text=\u00a0\u00bb191107 15.30 SS THERMALS MAP\u00a0\u00bb _builder_version=\u00a0\u00bb4.4.8″][\/et_pb_image][\/et_pb_column][et_pb_column type=\u00a0\u00bb1_4″ _builder_version=\u00a0\u00bb4.4.8″][et_pb_text _builder_version=\u00a0\u00bb4.4.8″]<\/p>\n Matthew Scutter had to modify his software to deal with ceilings above 8,000 m. The light W-NW flow to the west of the volcanoes line, and E-NE to the east of this line, on the Bolivian Altiplano, can be observed on this map. The converging front between these two air masses generates the \u00ab\u00a0Bolivian Winter\u00a0\u00bb, see below.<\/em><\/span><\/p>\n [\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=\u00a0\u00bb3_4,1_4″ _builder_version=\u00a0\u00bb4.4.8″][et_pb_column type=\u00a0\u00bb3_4″ _builder_version=\u00a0\u00bb4.4.8″][et_pb_image src=\u00a0\u00bbhttps:\/\/topfly-aero.com\/wp-content\/uploads\/2020\/06\/5E-191129-16.40-SS-X-SECTION.png\u00a0\u00bb title_text=\u00a0\u00bb5E 191129 16.40 SS X SECTION\u00a0\u00bb _builder_version=\u00a0\u00bb4.4.8″][\/et_pb_image][\/et_pb_column][et_pb_column type=\u00a0\u00bb1_4″ _builder_version=\u00a0\u00bb4.4.8″][et_pb_text _builder_version=\u00a0\u00bb4.4.8″]<\/p>\n Generating cross sections is an innovative function of SkySight. It also gives an idea of the altitude at which we can hope to catch the lift of the rebound (here 500 m AGL at the first rebound, i.e. 5,000 m MSL), and up to what altitude we can expect to climb and with what values, in this case more than 12,000 m at the 2nd rebound with up to 7 m\/s (verified!)<\/em><\/span><\/p>\n \u00a0<\/em><\/span><\/p>\n [\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=\u00a0\u00bb4.4.8″ custom_padding=\u00a0\u00bb3px|||||\u00a0\u00bb][et_pb_column type=\u00a0\u00bb4_4″ _builder_version=\u00a0\u00bb4.4.8″][et_pb_post_nav _builder_version=\u00a0\u00bb4.4.8″][\/et_pb_post_nav][\/et_pb_column][\/et_pb_row][\/et_pb_section]<\/p>\n","protected":false},"excerpt":{"rendered":" Was particularly successful, even if it took ten days to run in the system, ceilings of 7,000 to 8,000 m in thermal (most often blue) not being part of the meteorological standards. The forecast was limited to two days, sufficient for our goal, the discovery. The main interest of SkySight in thermals was the forecast […]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_et_pb_use_builder":"on","_et_pb_old_content":"","_et_gb_content_width":"1080","footnotes":""},"categories":[134],"tags":[],"class_list":["post-5314","post","type-post","status-publish","format-standard","hentry","category-atacama-2019-en"],"_links":{"self":[{"href":"https:\/\/topfly-aero.com\/index.php\/wp-json\/wp\/v2\/posts\/5314","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/topfly-aero.com\/index.php\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/topfly-aero.com\/index.php\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/topfly-aero.com\/index.php\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/topfly-aero.com\/index.php\/wp-json\/wp\/v2\/comments?post=5314"}],"version-history":[{"count":5,"href":"https:\/\/topfly-aero.com\/index.php\/wp-json\/wp\/v2\/posts\/5314\/revisions"}],"predecessor-version":[{"id":5324,"href":"https:\/\/topfly-aero.com\/index.php\/wp-json\/wp\/v2\/posts\/5314\/revisions\/5324"}],"wp:attachment":[{"href":"https:\/\/topfly-aero.com\/index.php\/wp-json\/wp\/v2\/media?parent=5314"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/topfly-aero.com\/index.php\/wp-json\/wp\/v2\/categories?post=5314"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/topfly-aero.com\/index.php\/wp-json\/wp\/v2\/tags?post=5314"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}